DocumentCode :
1605145
Title :
Radar subsurface sounding over the putative frozen sea in Cerberus Palus, Mars
Author :
Orosei, R. ; Cartacci, M. ; Cicchetti, A. ; Noschese, R. ; Federico, C. ; Frigeri, A. ; Flamini, E. ; Holt, J.W. ; Marinangeli, L. ; Pettinelli, E. ; Phillips, R.J. ; Picardi, G. ; Seu, R. ; Plaut, J.J.
Author_Institution :
Ist. Naz. di Astrofis., Ist. di Fis. dello Spazio Interplanetario, Rome, Italy
fYear :
2010
Firstpage :
1
Lastpage :
4
Abstract :
The area of Mars known as Cerberus Palus, suspected of harboring a frozen body of water, has been observed by the two subsurface sounding radar MARSIS and SHARAD. SHARAD data reveal subsurface interfaces at depths ranging from ~50 m to ~150 m which could be interpreted as either the bottom of an ice sheet lying over bedrock, or an interface between two lava flows. Echoes have been analyzed to estimate the dielectric properties of the surface layer, and results favor the interpretation that no ice is present in the area.
Keywords :
Mars; ground penetrating radar; planetary surfaces; remote sensing by radar; Cerberus Palus; MARSIS observations; Mars; SHARAD observations; dielectric properties; frozen sea; ground penetrating radar; ice sheet; lava flows; radar subsurface sounding; Airborne radar; Dielectric losses; Ice; Mars; Radar scattering; Radar tracking; Rough surfaces; Sea surface; Surface roughness; Surface topography; Mars; dielectric permittivity; ground penetrating radar; ice; lava flow; loss tangent;
fLanguage :
English
Publisher :
ieee
Conference_Titel :
Ground Penetrating Radar (GPR), 2010 13th International Conference on
Conference_Location :
Lecce
Print_ISBN :
978-1-4244-4604-9
Electronic_ISBN :
978-1-4244-4605-6
Type :
conf
DOI :
10.1109/ICGPR.2010.5550143
Filename :
5550143
Link To Document :
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